第三紀研究 的英文怎麼說

中文拼音 [dìsānjìyánjiū]
第三紀研究 英文
tertiary research
  • 第 : Ⅰ助詞（用在整數的數詞前 表示次序） auxiliary word for ordinal numbers Ⅱ名詞1 [書面語] （科第） gr...
  • 三 : Ⅰ數詞1. （二加一后所得） three 2. （表示多數或多次） more than two; several; many Ⅱ名詞（姓氏） a surname
  • 紀 : 紀名詞（姓氏） a surname
  • 研 : 研同 「硯」
  • 究 : Ⅰ動詞（仔細推求; 追查） study carefully; go into; investigate Ⅱ副詞[書面語] （到底; 究竟） actually; really; after all
  • 第三 : third第三帝國 [德國] the third reich （1934 1945）; 第三 （層）樓 [美國] third story; [英國] seco...
  • 研究 : 1. （探求） study; research 2. （考慮或商討） consider; discuss; deliberate
  1. In this paper, we investigated the fruits and seeds in detail from yunnan in the age of miocene and from shanxi in the age of pliocene. 1. a miocene flora of fruits and seeds is reported from a brown coal mine, named as mangdan, in western yunnan, sw china

    本論文首次對我國雲南和山西晚第三紀的果實和種子進行專門研究，並根據它們對應的現存最近親緣植物的分佈及生態特徵分析和重建了當時當地的古植被、古環境和古氣候。
  2. Zhang hong, wang yongdong, shen guanglong, he zonglian, wang jun. 1999, palaeophytogeography and palaeoclimatic implications of permian gigantopterids on the north china plate. proc. int. conf. pangea & palaeozoic transition. 167 - 168

    沈光隆，張泓，王軍，張雙全， 2000 ，陜西渭北煤田石炭-二疊紀植物地層初步研究，第三屆全國地層會議論文集。 117 - 124 。
  3. ( 4 ) the formation and growth of structural traps and stratigraphic - unconformity traps in the area is controlled by three compressive stages of silurian - devonian, late permian - tertiary and oligocene - quaternary ; non - structural and compound traps mainly grew in the early paleozoic. structural traps mostly grew in the late paleozoic and the cenozoic and mostly grew on the north and south belts ; non - structural traps mostly grew in the northern area of the hetian concave. most traps in the area formed or typed at last in the himalayan episode, dispersed on the north and south belts

    （ 4 ）研究區構造與地層不整合圈閉的形成和發育受志留-泥盆紀、晚二疊世-第三紀、漸新世-第四紀三個擠壓階段的控制；早古生代主要發育非構造圈閉和復合圈閉，晚古生代和新生代則主要發育構造圈閉：構造圈閉主要發育在南北兩帶上，其次為中帶；非構造圈閉主要發育在和田凹陷以北的地區；研究區內大多數圈閉是喜山期形成或最終定型的，在南北兩帶都有分佈，而海西期圈閉主要分佈於研究區中帶瑪南構造帶處。
  4. After analysis of some news and reports of economic daily and 21century economic report, the author discusses some problems of the successful persons ’ representation. the two newspapers always give person a kind of underrepresented images of “ successful persons ”. they are : 1 、 make the successful persons ’ record of formal schooling higher and make the images of the successful persons routinize. 2 、 the description of the successful persons is blurred. for example, it is not known how the successful persons got their first fortune. 3 、 the narration of the successful persons is routinized

    本文採用內容分析法對《經濟日報》人物版和《 21世紀經濟報道》的有關「成功人士」的報道進行再現研究，研究發現這兩家報紙對「成功人士」形象的再現出現偏差，主要表現在:一、將「新富人」階層學歷拔高，形象模式化;二、對于「成功人士」另「半張臉」的書寫模糊化，例如「成功人士」創業的「第一桶金」的來龍去脈隱晦不談;三、對于「成功人士」的敘事模式化。
  5. Through research, the organic matter of source rocks in carboniferous - permian coal measure strata began first hydrocarbon - generating in mesozoic, and the first hydrocarbon - filling took place. but, because of yanshan movement later, the carboniferous - permian strata rose, as a result, the first hydrocarbon - generating and reservoir - forming paused ; in early tertiary period, because carboniferous - permian strata dipping forward east originally turned into dipping forward west, the prototype of faulted block began to form gradually ; by the end of sha - 3 period of early tertiary, the paleogeotherm of carboniferous - permian strata exceed the mesozoic ' s temperature again, and accordingly, abundant hydrocarbon was generated and expulsed secondly. the trap continued to develop ; from the end of late tertiary to quaternary, the second hydrocarbon - generating and expulsing got to its peak, and the second reservoir - forming was over

    研究表明，本區石炭?二疊紀烴源巖在中生代發生一次生烴和排烴，並有油氣充注，后因燕山運動導致地層抬升，一次生烴和成藏過程中止；在早第三紀，原來東傾的地層變為西傾，斷塊圈閉開始具雛形；至早第三紀沙二末期，石炭?二疊系的大部分地層古地溫再次超過中生代一次生烴的溫度，開始二次生烴和排烴，圈閉持續發育；晚第三紀末?第四紀，二次生烴、排烴達到高峰，二次成藏完成。
  6. The qiantang basin, having the most complete and extensive marine sedimentary strata during jurassic, is the second larger mesozoic marine sedimentary basin. although many achievements are obtained in recent years, the research are still only involved in second - or third - order of mesozoic sequence. on the base of sedimentation facies analysis of matuo formation, high frequency sequence are studied

    藏北羌塘盆地地處青藏高原腹部，是我國中生代第二大海相沉積盆地，侏羅紀是羌塘盆地發育最全、分佈最廣泛的海相沉積層系近年來，羌塘盆地在層序地層方面的研究已取得不少成果，但其層序地層研究多涉及中生代二級或三級層序，至於高頻層序，尚未進行詳細的研究。
  7. According to the synthetically study of remnant stratum list, sediment system. character of sediment filling, comeback of archetypal basin and feature of tectonic deformation, santanghu basin passed through four formation and evolution phases : ( 1 ) formation and evolution of basin ' s basement ; ( 2 ) formation and evolution of fault - fold to depression basin in permian ; ( 3 ) formation and evolution of depression basin in triassic - jurassic - cretaceous ; (

    依據三塘湖盆地殘餘地層序列、沉積體系、沉積充填特徵和原型盆地恢復，以及不同構造層的構造變形特徵的綜合研究分析，認為三塘湖盆地經歷了如下四個發展演化階段：前二疊紀盆地基底發展演化階段；二疊紀斷陷-拗陷盆地發展演化階段； ：三疊-侏羅-白堊紀拗陷盆地發展演化階段；第三-第四系新生代盆地發展演化階段。
  8. Rotary centennial institute for wetland conservation district 3450 area 5 inaugurates

    扶輪百周年紀念濕地研究院三四五零區第五分域開幕
  9. Studies of geological samples from the kt boundary revealed the presence of c60

    從研究白堊紀，第三紀交接的地質樣本中找到碳- 60分子。
  10. Studies of geological samples from the k t boundary revealed the presence of c60

    從研究白堊紀，第三紀交接的地質樣本中找到碳- 60分子。
  11. Firstly, based on the basin prototype, the triassic and jurassic mudstone and coal, the main source rocks of the basin, did not develop better in baicheng sag than in the northern thrust belt including keyi structural belt ; secondly, because of the thrusting happened in late cenozoic, the triassic and jurassic source rocks reach to a high to over high maturity and thus generate gas or condensate oil mainly. thirdly, the thrust faults compelled the natural gas to migrate from the north to the south or from the deep to the shallow. as a result, the keyi structural belt and the eastern qiulitage structural belt enriched in natural gas because they were not only located on the migration routines of the natural gas, but also developed simultaneously when the gas migration happened

    從盆地構造史研究的角度認為庫車盆地的天然氣主要來源於北部山前沖斷帶： 1受原型盆地構造格局的制約，三疊系侏羅系烴源巖發育的最有利位置不是在拜城凹陷，而是在克依構造帶及其以北的北部山前沖斷帶2晚第三紀以來的逆沖推覆作用使得烴源巖提早進入高過成熟階段，並以產氣和凝析油為主3逆沖推覆作用所產生的北傾逆斷層控制天然氣自下而上自北而南運移，位於運移路線上的克依構造帶和秋里塔格構造帶的東段與烴源巖的排氣期匹配較好，從而使這些地區最富集天然氣。
  12. In a word, the stress field variation since mesozoic can be divided into five periods such as indosinian epoch, early yanshan epoch ( j3 - k1 ), end of yanshan epoch, eogene, neogene and quaternary, it is mainly affected by the active pattern of tanlu large fault

    綜合研究認為，本區自中生代以來的應力場變化可分為印支期、早燕山期（ j3 - k1 ） 、燕山末期、早第三紀、晚第三紀及第四紀五個階段，應力場的變化主要受郯廬大斷裂活動方式的影響。
  13. The neogene is a key stage of terrestrial environmental evolution in yunnan. three stratigraphic sections including luhe ( late miocene ), yangyi and longling ( late pliocene ) were selected to reconstruct vertical landscape of paleovegetation in these areas, based on palynological data. according to principle of the coexistence approach, seven quantitative paleoclimatic parameters of each deposit area were obtained by using meteorological data ( 1951 - 1980 ) of the distribution area of extant taxa found each palynoflora in china

    晚第三紀是雲南地區環境演變過程中的關鍵地質歷史時段，本論文以晚第三紀晚中新世（呂合） 、晚上新世（羊邑和龍陵）地層中的孢粉為研究對象，結合同層位大化石植物證據，參照現代植被，恢復了雲南三個化石出產地區的古植被垂直分佈景觀，並定性地描述了古氣候；同時運用共存分析方法（ theco - existenceapproach ）定量化地重建了三個地區的古氣候參數值；初步推測了沉積地可能的古海拔。
  14. The rotary centennial institute for wetland conservation district 3450 area 5 is a joint project of the five rotary clubs in rotary international district 3450 area 5 and world wide fund for nature hong kong wwf hong kong in commemoration of the 100th birthday of rotary international

    扶輪百周年紀念濕地研究院三四五零區第五分域下稱研究院為國際扶輪3450區第5分域的五個扶輪社下稱扶輪社與世界自然香港基金會下稱世界自然基金會的合作項目，以紀念國際扶輪成立一百周年。
  15. However, the ancient book zhu shu ji nian lei xue - xi first compiled and calibrated in the academic research history of the qing dynasty proves the value of zhu shu ji nian as historical data which compensates for records of the historian in recording the ancient history of the three dynasties

    但他在清代學術研究史上第一次輯錄、校訂古本《竹書紀年》 ，並極力為其正名，肯定其史料價值足以彌補《史記》等書關於三代古史記載的缺陷。
  16. Nw compressive structures are developed in indosinian epoch in which folds are predominant and companied with some small thrusts. nearly ns or nnw compressive structures are developed at the end of yanshan epoch in which it is mainly overthrusted structures and closed folded structures. large gentle anticlines and synclines are developed from the end of mesozoic to early tertiary, and antithetic sagging structures are developed in mesozoic

    研究發現，本區印支期發育了以褶皺為主、局部伴有小型逆斷層的北西向壓性構造，燕山末期（中生代末期）發育了以逆掩構造和緊閉的褶皺構造為主的近南北向或北北西向壓性構造，中生代末到第三紀早期發育了以寬緩為特徵的大型背斜向斜構造，以及中生界內部的逆牽引構造。
  17. Based on the study of the test pressure data, the acoustic time and the reconstrction of paleoformation pressure, through the study of abnormal pressure in the middle and western sichuan basin, it ' s shown that the distribution of stratum pressure differs greatly in different zones ; the evolution history of paleo - formation pressure has been restored according to the models of the evolution history of pressure, and it shows that there were two high pressure arouse, the first arouse in later jurassic and the second in erlier triassic, analyzing the relations between the excessive pressure distribution and the petroleum migration

    摘要通過實測壓力數據、泥巖聲波壓實研究、古壓力恢復研究，對川西、川中地區異常壓力在縱向、橫向上的分佈特點的分析，認?該區異常壓力分佈有明顯的分區性；同時，依據異常壓力的孕育史模型，恢復本地區的上三疊統古壓力的形成與演化歷史，認?上三疊統過剩壓力高峰出現過兩次，分別在晚侏羅世末和早第三紀末；最後分析了該區異常壓力與油氣運聚的關系。
  18. ( 5 ) according to the study on seismicic data, sedimentary characteristics, contact relations, incision relation of the faults and strata related to the folds which are associated with the faults, this paper reached the conclusions : the oblique - thrusting structure of sertengshan - xitieshan in northern qaidam basin was formed in middle jurassic and the left - thrusting fault zone was established in the late pliocene of neogene

    （ 5 ）根據地震質料、沉積特徵、地層的沉積接觸關系、斷裂切割地層關系以及與斷裂相關的褶皺捲入地層的研究，認為柴達木盆地北緣的賽什騰? ?錫鐵山逆沖推覆構造形成於中侏羅世，而左行逆沖斷裂帶定型于新第三紀上新世末。
  19. Under the guide of dynamic system for pool - forming and petroleum system, this research has fully taken advantage of every kinds of data from the area, applied the new idea, new technology, new methods to study tectonic, sedimentary and resource rock. the results suggest that the source rock of permo - carboniferous has undergone three evolution periods. the first gas generation occurs at the end of triassic and the generation stopped during jurassic - cretaceous

    該文以成藏動力學系統和含油氣系統理論為指導，充分利用工區以及鄰區的各種資料，運用新思路、新技術、新方法，在構造、沉積、烴源巖評價等基礎地質研究的基礎上，認為石炭?二疊系烴源巖經歷了三疊紀末期以前的一次生氣階段、侏羅紀?白堊紀時期的演化停止階段和早第三紀至今的二次生氣階段等三個階段。
  20. The volume of diffusion gas has been calculated with the application for the pick ' s theorem to the local geological features, which proved that the gasfiields formed before tertiary has entirely been destroyed. it is concluded that medium or small gas - pools might be found in the depression. finally, the paper proposes some plays

    特別是，以菲克定律為基礎，結合研究區的實際地質條件，嘗試性地通過計算證明，第三紀以前形成的氣藏（一次成烴階段）已被破壞，散失殆盡，二次成烴（第三紀以後）具備形成中?小型氣田的基本地質條件，具有良好的勘探前景。
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